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{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,9,16]],"date-time":"2024-09-16T16:24:14Z","timestamp":1726503854182},"reference-count":113,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2009,1,1]],"date-time":"2009-01-01T00:00:00Z","timestamp":1230768000000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["SP"],"published-print":{"date-parts":[[2009,1]]},"abstract":"Abstract<\/jats:title>\n New field data on the East Mediterranean domain suggest that this oceanic basin belonged to the larger Neotethyan oceanic system that opened in Permian times. A Greater Apulia domain existed in Mesozoic times, including the autochthonous units of Greece and SW Turkey. It also included a united Adria and Apulia microplate since Early Jurassic times. This key information implies that a new post-Variscan continental fit for the western Tethyan area is necessary, where the relationships between the Adriatic, Apulian and Iberian plates are defined with greater confidence. To construct a reliable palinspastic model of the Alpine realm, plate tectonic constraints must be taken into consideration in order to assess the magnitude of lateral displacements. For most of the plates and their different terranes, differential transport on the scale of thousands of kilometres can be demonstrated. This plate tectonic framework allows a better geodynamic scenario for the formation of the Alpine chain to be proposed, where the western and eastern transects have experienced contrasting geological evolutions. The eastern Alps\u2013Carpathians domain evolved from the north-directed roll-back of the Maliac\u2013Meliata slab and translation of the Meliata suture and Austroalpine domain into the Alpine domain. In the western Alps, the changing African plate boundary in space and time defined the interaction between the Iberian\u2013Brian\u00e7onnais plate and the Austroalpine accretionary wedge.<\/jats:p>","DOI":"10.1144\/sp327.6","type":"journal-article","created":{"date-parts":[[2009,12,21]],"date-time":"2009-12-21T19:49:52Z","timestamp":1261424992000},"page":"89-111","source":"Crossref","is-referenced-by-count":120,"title":["Plate tectonics of the Alpine realm"],"prefix":"10.1144","volume":"327","author":[{"given":"G\u00e9rard M.","family":"Stampfli","sequence":"first","affiliation":[{"name":"Institute of Geology and Palaeontology, University of Lausanne, Anthropole, CH 1015 Lausanne, Switzerland"}]},{"given":"Cyril","family":"Hochard","sequence":"additional","affiliation":[{"name":"Institute of Geology and Palaeontology, University of Lausanne, Anthropole, CH 1015 Lausanne, Switzerland"}]}],"member":"1881","published-online":{"date-parts":[[2009,12,21]]},"reference":[{"issue":"3","key":"e_1_3_2_2_1","first-page":"641","article-title":"Le flysch de la nappe du Niesen","volume":"79","author":"Ackermann A.","year":"1986","unstructured":"Ackermann A.Le flysch de la nappe du NiesenEclogae geologicae Helvetiae1986793641684","journal-title":"Eclogae geologicae Helvetiae"},{"key":"e_1_3_2_3_1","first-page":"47","article-title":"The Northern Apennines and the kinematics of Africa \u2013 Europe Convergence","volume":"1","author":"Argnani A.","year":"2002","unstructured":"Argnani A.The Northern Apennines and the kinematics of Africa \u2013 Europe ConvergenceBolletino della Societ\u00e0 Geologica Italiana, Volume Speciale200214760","journal-title":"Bolletino della Societ\u00e0 Geologica Italiana, Volume Speciale"},{"key":"e_1_3_2_4_1","first-page":"735","volume-title":"PeriTethys Memoir 6: Peritethyan Rift\/wrench Basins and Passive Margins, IGCP 369","author":"Argnani A.","year":"2001","unstructured":"Argnani A., Savelli C., Ziegler P. 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